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中国大宝山矿酸性矿山排水中的古菌多样性。

Archaeal diversity in acid mine drainage from Dabaoshan Mine, China.

作者信息

Qiu Guan-Zhou, Wan Min-Xi, Qian Lin, Huang Zhi-Ying, Liu Kai, Liu Xue-Duan, Shi Wu-Yang, Yang Yu

机构信息

School of Minerals Processing and Bioengineering, Central South University, Changsha, Hunan, China.

出版信息

J Basic Microbiol. 2008 Oct;48(5):401-9. doi: 10.1002/jobm.200800002.

Abstract

Three acid mine drainage (AMD) samples collected from Dabaoshan Mine (Guangdong Province, China) were studied. In addition to physicochemical analyses, the diversity and community structures of the archaeal communities in these samples were described at the genetic level by amplified ribosomal DNA restriction analysis (ARDRA). Nine different ARDRA patterns were obtained from 146 clones and were studied as operational taxonomic units (OTUs), which were re-amplified and sequenced. Sequence data and phylogenetic analysis showed that most of the clones belonged to the Thermoplasmatales, and that archaea belonging to the Sulfolobales were absent. Only 1 OTU attributed to Ferroplasma was found and was observed to be abundant in all 3 samples. Eight OTUs were related to 2 new undefined groups in the Thermoplasmatales. Of the 8 OTUs, the clones in 2 similar units were isolated from samples collected from an abandoned sulfide mine (Huelva, Spain) and those in 5 similar units were isolated from samples collected from a closed copper mine (Tonglushan, China). These diversities were characterized by the reciprocal of Simpson's index (1/D) and correlated with the concentrations of ferrous ions and toxic ions in the AMD samples. The high temperature of the sampling sites was one of the factors that could explain why archaea belonging to the Thermoplasmatales were abundant in the analyzed AMD samples while those belonging to the Sulfolobales were absent.

摘要

对从中国广东省大宝山矿采集的三个酸性矿山排水(AMD)样本进行了研究。除了理化分析外,还通过扩增核糖体DNA限制性分析(ARDRA)在基因水平上描述了这些样本中古菌群落的多样性和群落结构。从146个克隆中获得了9种不同的ARDRA模式,并将其作为操作分类单元(OTU)进行研究,对这些OTU进行了重新扩增和测序。序列数据和系统发育分析表明,大多数克隆属于嗜热栖热菌目,且不存在属于硫化叶菌目的古菌。仅发现了1个归属于铁原体属的OTU,且在所有3个样本中均观察到其丰度较高。8个OTU与嗜热栖热菌目中2个新的未定义类群相关。在这8个OTU中,2个相似单元中的克隆是从西班牙韦尔瓦一个废弃硫化矿采集的样本中分离得到的,5个相似单元中的克隆是从中国铜绿山一个封闭铜矿采集的样本中分离得到的。这些多样性以辛普森指数的倒数(1/D)来表征,并与AMD样本中的亚铁离子和有毒离子浓度相关。采样点的高温是可以解释为什么在分析的AMD样本中嗜热栖热菌目的古菌丰富而硫化叶菌目的古菌不存在的因素之一。

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